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南加州地壳的伴随层析成像

Adjoint tomography of the southern California crust.

作者信息

Tape Carl, Liu Qinya, Maggi Alessia, Tromp Jeroen

机构信息

Seismological Laboratory, California Institute of Technology, Pasadena, CA 91125, USA.

出版信息

Science. 2009 Aug 21;325(5943):988-92. doi: 10.1126/science.1175298.

Abstract

Using an inversion strategy based on adjoint methods, we developed a three-dimensional seismological model of the southern California crust. The resulting model involved 16 tomographic iterations, which required 6800 wavefield simulations and a total of 0.8 million central processing unit hours. The new crustal model reveals strong heterogeneity, including local changes of +/-30% with respect to the initial three-dimensional model provided by the Southern California Earthquake Center. The model illuminates shallow features such as sedimentary basins and compositional contrasts across faults. It also reveals crustal features at depth that aid in the tectonic reconstruction of southern California, such as subduction-captured oceanic crustal fragments. The new model enables more realistic and accurate assessments of seismic hazard.

摘要

我们采用基于伴随方法的反演策略,构建了南加州地壳的三维地震模型。最终模型历经16次层析成像迭代,这需要进行6800次波场模拟,总共耗费80万个中央处理器小时。新的地壳模型显示出强烈的非均匀性,相对于南加州地震中心提供的初始三维模型,局部变化达±30%。该模型揭示了诸如沉积盆地等浅层特征以及断层两侧的成分差异。它还展现了深部地壳特征,有助于对南加州进行构造重建,比如俯冲捕获的大洋地壳碎片。新模型能够对地震危险性进行更现实、准确的评估。

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